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- W2083230854 abstract "Abstract A simple physical model, the thickening plate model, gives a possible explanation of the fact that the averaged terrestrial heat flow over oceans and continents is roughly equal. In the model, latent heat released by solidification of asthenospheric material plays an important role: faster development (thickening) of oceanic lithosphere releases a larger amount of latent heat than does continental lithosphere, and the heat production becomes comparable with radiogenic heat production within continental crust. The model also suggests that the rough equality of the heat flows is not an essential feature of the Earth but merely coincidental under the conditions of the present plate motion. A more important feature may be the similarity of the terrestrial heat flow over the oldest regions of both continents and oceans. Terrestrial heat flow over an oceanic area may be a function of the spreading rate of the lithosphere: if the spreading rate of the organic lithosphere is slower than the present rate, the averaged terrestrial heat flow over oceans should be lower." @default.
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- W2083230854 date "1989-08-01" @default.
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- W2083230854 title "A hypothesis on the heat flow similarity between oceans and continents" @default.
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- W2083230854 doi "https://doi.org/10.1016/0040-1951(89)90013-9" @default.
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